Chapter 10, Lesson 6
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The document discusses various weather-related terms including wind, convection cells, sea and land breezes, the Coriolis effect, instruments like hygrometers and barometers, and high and low pressure systems. It provides definitions for key concepts like convection cells, sea and land breezes, isobars, and how high and low pressure systems impact weather conditions.
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Air pressure changes with temperature and elevation. Warmer air is less dense and rises, creating low pressure areas, while cooler air is denser and sinks, creating high pressure areas. Wind is caused by air moving from high to low pressure areas. Air pressure is measured with a barometer, wind direction with a wind vane, and wind speed with an anemometer. For a set of daily wind speed data, the range is the difference between the highest and lowest values, the median is the middle number after sorting, and the mode is the number that occurs most frequently.
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Air pressure is the force exerted by the weight of air above a given point. A barometer is an instrument that measures air pressure, with mercury levels rising and falling based on increases and decreases in pressure. Wind results from differences in air pressure as air moves from high to low pressure areas. Solar radiation ultimately drives wind by unevenly heating the Earth's surface and generating pressure gradients. The Coriolis effect causes deflection of moving objects and winds right in the Northern Hemisphere and left in the Southern Hemisphere due to the Earth's rotation.
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A Bermuda High is a high-pressure air system that forms along the East Coast and causes heat waves. The downward force from the high pressure system pushes out cooler air and prevents cooler air fronts from breaking through, keeping temperatures warm. This high pressure system rotates like a cylinder and increases the air pressure through torque, similarly to how a helicopter's propellers create downward draft. Warm, moist air from the Caribbean sustains this high pressure system and prolongs the heat.
Air pressure
1) A planet's atmosphere is determined by its gravity - large planets with strong gravity can hold thicker atmospheres than low-mass planets with weak gravity.
2) Atmospheric pressure depends on the thickness of the atmosphere, which is influenced by a planet's gravity. Stronger gravity holds more gas and increases atmospheric pressure.
3) On Earth, atmospheric pressure is measured using barometers. The mercury barometer measures air pressure through the height mercury is pushed up in a glass tube by atmospheric pressure. The aneroid barometer uses changes in the pressure on an evacuated metal cell to measure air pressure without toxic mercury.
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Pressure is determined by the force acting on a surface area. It depends on two factors - the force applied and the area over which that force is spread. Pressure increases with greater force or smaller surface area. In liquids, pressure is transmitted equally in all directions and increases with depth. Atmospheric pressure from gases also increases when the temperature is higher or when there is more air/gas content. Instruments like mercury barometers and manometers can be used to measure gas and liquid pressures.
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This document defines key vocabulary terms related to weather and climate, including weather, atmosphere, climate, precipitation, wind, anemometer, meteorologist, and wind vane. It explains that weather is the current atmospheric conditions, atmosphere is the air surrounding Earth, and climate is the combination of weather over time in a region. Precipitation refers to rain, snow or hail falling to the surface. An anemometer measures wind speed and a wind vane measures wind direction. Meteorologists are scientists who study weather and the atmosphere.
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Air pressure changes with temperature and elevation. Warmer air is less dense and rises, creating low pressure areas, while cooler air is denser and sinks, creating high pressure areas. Wind is caused by air moving from high to low pressure areas. Air pressure is measured with a barometer, wind direction with a wind vane, and wind speed with an anemometer. For a set of daily wind speed data, the range is the difference between the highest and lowest values, the median is the middle number after sorting, and the mode is the number that occurs most frequently.
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Air pressure is the force exerted by the weight of air above a given point. A barometer is an instrument that measures air pressure, with mercury levels rising and falling based on increases and decreases in pressure. Wind results from differences in air pressure as air moves from high to low pressure areas. Solar radiation ultimately drives wind by unevenly heating the Earth's surface and generating pressure gradients. The Coriolis effect causes deflection of moving objects and winds right in the Northern Hemisphere and left in the Southern Hemisphere due to the Earth's rotation.
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A Bermuda High is a high-pressure air system that forms along the East Coast and causes heat waves. The downward force from the high pressure system pushes out cooler air and prevents cooler air fronts from breaking through, keeping temperatures warm. This high pressure system rotates like a cylinder and increases the air pressure through torque, similarly to how a helicopter's propellers create downward draft. Warm, moist air from the Caribbean sustains this high pressure system and prolongs the heat.
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1) A planet's atmosphere is determined by its gravity - large planets with strong gravity can hold thicker atmospheres than low-mass planets with weak gravity.
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3) On Earth, atmospheric pressure is measured using barometers. The mercury barometer measures air pressure through the height mercury is pushed up in a glass tube by atmospheric pressure. The aneroid barometer uses changes in the pressure on an evacuated metal cell to measure air pressure without toxic mercury.
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Pressure is determined by the force acting on a surface area. It depends on two factors - the force applied and the area over which that force is spread. Pressure increases with greater force or smaller surface area. In liquids, pressure is transmitted equally in all directions and increases with depth. Atmospheric pressure from gases also increases when the temperature is higher or when there is more air/gas content. Instruments like mercury barometers and manometers can be used to measure gas and liquid pressures.
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The document summarizes the history of meteorology and invention of weather instruments. It describes how early weather observation relied on simple sky observations. The barometer was invented in 1643, allowing air pressure to be measured. The hygrometer for humidity followed in 1644. Daily weather measurements began in 1765 in France. Modern meteorology emerged from storm analyses in the 1850s. New instruments like weather satellites and numerical weather models now provide highly accurate forecasts. Key weather instruments are also summarized, including who invented the barometer, anemometer, hygrometer, rain gauge and thermometer. Cloud types are named based on the pioneering work of Luke Howard in the early 1800s.
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This document discusses atmospheric pressure and how it is measured. It defines atmospheric pressure as the force per unit area exerted by the entire air mass above a specified surface. Atmospheric pressure can be measured using a mercury barometer or an aneroid barometer. It describes how pressure decreases with increasing altitude and discusses standard atmospheric pressure units and how pressure varies globally and with weather patterns.
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Here are the key steps to solve these atmospheric pressure and boiling point calculation problems:
1) H = 11(760 - 721) = 429 m
2) H = 4,070 m, P = 760 - (H/11) = 760 - (4,070/11) = 390 mm Hg
3) H = 2,376 m, B.P. = 100 - (760 - P)/27 = 100 - (760 - (760 - (H/11)))/27 = 100 - (760 - (760 - (2,376/11)))/27 = 95 °C
4) P = 625 mm Hg, H = 11(760 - P) = 11(
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Isobars that are close together indicate strong winds due to a large pressure difference over a small area, while isobars farther apart show gentler winds from a smaller pressure change. Isobars also show locations of high and low pressure areas. Air pressure decreases with increasing altitude as there are fewer air molecules, and high and low pressure systems affect incoming weather, with high pressure typically bringing cooler and clearer conditions and low pressure often accompanying warmer temperatures, storms and rain.
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This document defines key terms related to air pressure and wind, including wind, convection cells, sea breeze, land breeze, Coriolis effect, and isobar. It explains that convection cells are patterns of rising and falling air caused by uneven heating and cooling of the air. A sea breeze blows from the sea to land, while a land breeze goes from land to sea. The Coriolis effect causes winds to curve right in the northern hemisphere and left in the southern hemisphere. Isobars connect points of equal air pressure on a map.
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Air pressure is exerted equally in all directions by the air around us. It can be measured using a barometer, with units of mmHg or atm. Rapid changes in air pressure often indicate approaching weather systems - falling pressure means storms while rising pressure means clearing weather. Winds are created by differences in air pressure between areas. Global wind patterns are caused by uneven heating of the Earth, with the hottest air at the equator rising and causing circulation of air masses. High and low pressure systems form based on temperature and moisture levels, influencing wind direction.
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Uneven heating of the atmosphere causes warm air to rise and cool air to sink, generating wind as air moves from high to low pressure areas. The Coriolis effect causes objects in the northern hemisphere to be deflected to the right and objects in the southern hemisphere to be deflected to the left as the Earth rotates. Global wind patterns include trade winds near the equator, prevailing westerlies at mid-latitudes, and polar easterlies near the poles. Jet streams are fast winds in the upper atmosphere that can help or hinder airplane travel. Air masses originate over land or water and bring the characteristic weather of their source region when they move over new areas. Different types of fronts form boundaries between air masses
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Here are the key steps to solve these atmospheric pressure and boiling point calculation problems:
1) H = 11(760 - 721) = 429 m
2) H = 4,070 m, P = 760 - (H/11) = 760 - (4,070/11) = 390 mm Hg
3) H = 2,376 m, B.P. = 100 - (760 - P)/27 = 100 - (760 - (760 - (H/11)))/27 = 100 - (760 - (760 - (2,376/11)))/27 = 95 °C
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1) Insolation refers to the amount of solar radiation that reaches Earth from the Sun at a given place and time.
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Air pressure is exerted equally in all directions by the air around us. It can be measured using a barometer, with units of mmHg or atm. Rapid changes in air pressure often indicate approaching weather systems - falling pressure means storms while rising pressure means clearing weather. Winds are created by differences in air pressure between areas. Global wind patterns are caused by uneven heating of the Earth, with the hottest air at the equator rising and causing circulation of air masses. High and low pressure systems form based on temperature and moisture levels, influencing wind direction.
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The document discusses ocean currents and their impact on climate. It explains that warm surface currents originate near the equator and flow north, while cool surface currents originate in northern regions and flow south. The currents curve due to the Coriolis effect caused by the Earth's rotation. Ocean currents affect climate by moderating temperatures - warm currents bring warmer temperatures to cool climates, while cool currents have the opposite effect. Being near large bodies of water also helps regulate land temperatures.
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The document discusses pressure in liquids and gases. It defines pressure as force per unit area and describes how pressure increases with depth in liquids. Pressure in liquids depends on depth, density and is independent of container shape. Atmospheric pressure varies with height and acts in all directions. Gas pressure is caused by molecular collisions with container walls. Instruments like barometers are used to measure atmospheric and gas pressures.
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The document discusses concepts related to hydrostatics and pressure, including:
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- The definition of pressure as force over area
- Factors that pressure depends on, such as force, area, and their relationships
- Applications of pressure concepts like sharp knives cutting better and ice skates gripping ice
- Pascal's principle and its demonstration using a syringe and hydraulic press
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Isobars that are close together indicate strong winds due to a large pressure difference over a small area, while isobars farther apart show gentler winds from a smaller pressure change. Isobars also show locations of high and low pressure areas. Air pressure decreases with increasing altitude as there are fewer air molecules, and high and low pressure systems affect incoming weather, with high pressure typically bringing cooler and clearer conditions and low pressure often accompanying warmer temperatures, storms and rain.
Weather tools
This document discusses common weather tools, including thermometers for measuring temperature, wind vanes for determining wind direction, anemometers for measuring wind speed, barometers for air pressure readings that can predict weather, and rain gauges for collecting rainfall measurements. Each tool plays an important role in weather observation and prediction.
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This document defines key vocabulary words related to weather including: weather, atmosphere, temperature, front, wind, anemometer, meteorologist, and weather map. It explains that weather is the happenings in the atmosphere at a certain time, and defines atmosphere as the air surrounding Earth. It also provides short definitions for temperature, front, wind, anemometer, meteorologist, and weather map.
SPM Physics - Solid and fluid pressure
Solid pressure is defined as the force acting on a given area, measured in Pascals. Fluid pressure results from particle collisions within the fluid and increases with depth and density. It is described by the equation P=hρg. Atmospheric pressure decreases with altitude and is measured using barometers. Fluids transfer pressure equally in all directions according to Pascal's principle, which has applications in hydraulic systems. Archimedes' principle describes buoyancy as the upward force equal to the weight of fluid displaced. Bernoulli's principle states that fluid pressure decreases where velocity increases, as seen in aerofoils, venturi nozzles, and other streamlined objects.
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Similar to Chapter 10, Lesson 6
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This document defines key terms related to air pressure and wind, including convection cells, sea breezes, land breezes, the Coriolis effect, isobars, and various instruments used to measure weather conditions like hygrometers, thermometers, and barometers. It also explains that convection cells cause rising and falling air and winds through the uneven heating and cooling of air, while sea breezes and land breezes are winds that blow from the sea to land or land to sea respectively.
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This document defines key terms related to air pressure and wind, including wind, convection cells, sea breeze, land breeze, Coriolis effect, and isobar. It explains that convection cells are patterns of rising and falling air caused by uneven heating and cooling of the air. A sea breeze blows from the sea to land, while a land breeze goes from land to sea. The Coriolis effect causes winds to curve right in the northern hemisphere and left in the southern hemisphere. Isobars connect points of equal air pressure on a map.
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Air pressure is exerted equally in all directions by the air around us. It can be measured using a barometer, with units of mmHg or atm. Rapid changes in air pressure often indicate approaching weather systems - falling pressure means storms while rising pressure means clearing weather. Winds are created by differences in air pressure between areas. Global wind patterns are caused by uneven heating of the Earth, with the hottest air at the equator rising and causing circulation of air masses. High and low pressure systems form based on temperature and moisture levels, influencing wind direction.
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Uneven heating of the atmosphere causes warm air to rise and cool air to sink, generating wind as air moves from high to low pressure areas. The Coriolis effect causes objects in the northern hemisphere to be deflected to the right and objects in the southern hemisphere to be deflected to the left as the Earth rotates. Global wind patterns include trade winds near the equator, prevailing westerlies at mid-latitudes, and polar easterlies near the poles. Jet streams are fast winds in the upper atmosphere that can help or hinder airplane travel. Air masses originate over land or water and bring the characteristic weather of their source region when they move over new areas. Different types of fronts form boundaries between air masses
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Ch 19 v2
1. The highest recorded wind speed occurred in Mount Washington, New Hampshire in 1934 at 372 km/h.
2. Air pressure is the force exerted by the weight of air above and is measured using a barometer. It affects wind, temperature, humidity and weather forecasting.
3. Differences in air pressure cause wind, with air flowing from high to low pressure areas. The rotation of the Earth causes the Coriolis effect which deflects winds right in the Northern Hemisphere.
Chapter 19
1. The highest recorded wind speed occurred in Mount Washington, New Hampshire in 1934 and was 372 km/h.
2. Air pressure is the pressure exerted by the weight of the air above and is measured using a barometer. It affects wind, temperature, humidity and weather forecasting.
3. Differences in air pressure cause wind to flow from high to low pressure areas, and the rotation of the Earth causes winds to be deflected via the Coriolis effect.
Chapter 19notes
1. The highest recorded wind speed occurred in Mount Washington, New Hampshire in 1934 at 372 km/h.
2. Air pressure is the pressure exerted by the weight of the air above and is measured using a barometer. Changes in air pressure can cause changes in wind, humidity, temperature, and affect weather forecasting.
3. Wind is caused by differences in air pressure and is influenced by factors like the pressure gradient, Coriolis effect, and friction near the Earth's surface.
Ch.19 Notes Mc Neely 2009
1. Air pressure is caused by the weight of air above exerting pressure in all directions, and differences in air pressure cause wind as air moves from high to low pressure areas.
2. Global wind patterns are caused by uneven heating of the Earth's surface by the sun, which causes large scale rising and sinking of air and the formation of circulation cells.
3. Local winds like sea breezes and valley winds are caused by smaller scale differences in air pressure caused by uneven heating of land and water areas.
Babelene@powerpoint
Meteorology is the scientific study of the atmosphere and weather forecasting. It has developed significantly since the 18th century with the establishment of observation networks across many countries. Further breakthroughs in weather forecasting occurred in the late 20th century with the development of computers. Meteorology studies observable weather events and phenomena through measurements of atmospheric variables like temperature, pressure, and water vapor at different spatial scales from local to global. It is closely related to other atmospheric sciences and has applications across diverse fields.
Babelene
Meteorology is the scientific study of the atmosphere and weather forecasting. It has developed significantly since the 18th century with the establishment of observation networks across many countries. Further breakthroughs in weather forecasting occurred in the late 20th century with the development of computers. Meteorology studies observable weather events and phenomena through measurements of atmospheric variables like temperature, pressure, and water vapor at different spatial scales from local to global. It is closely related to other atmospheric sciences and has applications across diverse fields.
Babelene
Meteorology is the scientific study of the atmosphere and weather forecasting. Significant advances occurred in the 18th century with observing networks, and in the 20th century with the development of computers enabling improved weather forecasting. Meteorology studies temperature, pressure, water vapor and how they interact and change over time at various spatial scales from local to global. It is related to other atmospheric sciences and has applications across many fields. Common weather instruments measure rainfall, temperature, pressure, wind speed and direction, sunshine, and humidity.
Air pressure
Air pressure is the weight of the atmosphere pressing down on the earth. It is measured in units called millibars using a barometer, which often contains mercury in a glass column like a thermometer to measure changes in pressure.
Geography Elective/Pure: Weather and climate notes
This is the notes and slides provided and compiled by teachers from reputable schools. Took me many months to compile this and share with you guys! By the way, the slides with a star usually mean that it will be significant so take note! Sharing with you now is this notes!!! Enjoy and love geography!!!
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The document discusses various weather elements and climate concepts. It defines weather as the short-term atmospheric conditions of a place, while climate refers to the average weather conditions over a long period, typically 30 years. It then describes different weather elements such as temperature, rainfall, relative humidity, wind, and cloud cover. It explains how these elements are measured and influenced by various factors like latitude, altitude, distance from the sea, and cloud cover. The document also discusses different climate types including equatorial, monsoon, and cool temperate climates. It examines evidence that the global climate is changing due to natural and human-induced causes such as increasing greenhouse gas emissions.
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The document discusses the key components and layers of the Earth's atmosphere. It notes that the atmosphere begins at the planet's surface and extends upwards approximately 1,000 km. It is composed primarily of oxygen, nitrogen, and other gases like argon and carbon dioxide. The atmosphere protects the Earth from the sun's rays and weather phenomena occur in its lower layers. It then provides more details on the specific atmospheric layers including the troposphere, stratosphere, mesosphere, thermosphere, and exosphere.
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This document defines and describes several key atmospheric variables:
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Chapter 10, Lesson 6
- 1. wind convection cells sea breeze land breeze Coriolis effect isobar hygrometer thermometer rain gauge weather vane anemometer barometer high pressure system low pressure system Air Pressure and Wind Chapter 10, Lesson 6
- 2. wind – air that moves horizontally
- 3. convection cell – a pattern of rising and falling air, sinking air, and winds caused by unequal heating and cooling of the air
- 4. convection cell – a pattern of rising and falling air, sinking air, and winds caused by unequal heating and cooling of the air
- 5. convection cell – a pattern of rising and falling air, sinking air, and winds caused by unequal heating and cooling of the air
- 6. sea breeze – a wind that blows from the sea toward the land
- 7. sea breeze – a wind that blows from the sea toward the land
- 8. land breeze – a wind that blows from the land toward the sea
- 9. sea breezes vs. land breezes
- 10. Coriolis effect – no matter which way the wind blows, it will always pull toward the right in the northern hemisphere, and to the left in southern hemisphere.
- 11. Coriolis effect – no matter which way the wind blows, it will always pull toward the right in the northern hemisphere, and to the left in southern hemisphere.
- 12. isobar – a line on a map connecting places with equal air pressure
- 13. hygrometer - an instrument that measures relative humidity.
- 14. thermometer - an instrument that measures temperature
- 15. rain gauge - an instrument that measures temperature
- 16. weather vane- an instrument that wind direction
- 17. anemometer - an instrument that measures wind SPEED
- 18. barometer - an instrument that measures air pressure
- 19. low pressure system- a weather system that usually brings rainy weather.
- 20. high pressure system – a weather system that brings fair weather.